| Summary: | The stable carbon isotope composition of particulate organic carbon (δ13CPOC) and naturally occurring long-lived radionuclide 226Ra (T1/2=1600a) were applied to study the variations of upper ocean (13CPOC values ranged from -27.4‰ to -19.0‰ and generally decreased from inner bay (south of 67°S) toward the Antarctic Divergence. Surface water 226Ra activity concentration ranged from 0.92 to 2.09Bq/m3 (average 1.65±0.32Bq/m3, n=20) and increased toward the Antarctic Divergence, probably reflecting the influence of 226Ra-depleted meltwater and upwelled 226Ra-replete deep water. The fraction of meltwater, fi, was estimated from 226Ra activity concentration and salinity using a three-component (along with Antarctic Summer Surface Water, and Prydz Bay Deep Water) mixing model. Although the fraction of meltwater is relatively minor (1.6-11.9%, average 4.1±2.7%, n=20) for the surface waters (sampled at ~6m), a positive correlation between surface δ13CPOC and fi (δ13CPOC=0.94×fi-28.44, n=20, r2=0.66, p13CPOC values in the inner Prydz Bay compared to the open oceanic waters. This is the first time for a relationship between δ13CPOC and meltwater fraction to be reported in polar oceans to our knowledge. We propose that sea ice melting may have affected surface ocean δ13CPOC by enhancing water column stability and providing a more favorable light environment for phytoplankton photosynthesis, resulting in drawdown of seawater CO2 availability, likely reducing the magnitude of isotope fractionation during biological carbon fixation. Our results highlight the linkage of ice melting and δ13CPOC, providing insights into understanding the carbon cycling in the highly productive Antarctic waters. ? 2013 Elsevier Ltd.
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